Radiometric validation of the Atmospheric Infrared Sounder over the Antarctic Plateau
[1] Validation of infrared satellite instruments, after they have been launched into orbit, has traditionally relied on views of the relatively warm sea surface. The Antarctic Plateau provides a complementary validation target from space because it is also homogeneous over large areas, yet it is rel...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.524.6761 2023-05-15T13:59:34+02:00 Radiometric validation of the Atmospheric Infrared Sounder over the Antarctic Plateau The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.6761 http://www.webpages.uidaho.edu/~vonw/pubs/waldenetal_2006.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.6761 http://www.webpages.uidaho.edu/~vonw/pubs/waldenetal_2006.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.webpages.uidaho.edu/~vonw/pubs/waldenetal_2006.pdf text ftciteseerx 2016-01-08T10:18:11Z [1] Validation of infrared satellite instruments, after they have been launched into orbit, has traditionally relied on views of the relatively warm sea surface. The Antarctic Plateau provides a complementary validation target from space because it is also homogeneous over large areas, yet it is relatively cold. During summer, cloud-free conditions occur often and the atmospheric humidity is very low with values of total column water vapor around 1 mm. Radiance validation experiments were conducted at Text Antarc* Antarctic Unknown Antarctic The Antarctic |
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ftciteseerx |
language |
English |
description |
[1] Validation of infrared satellite instruments, after they have been launched into orbit, has traditionally relied on views of the relatively warm sea surface. The Antarctic Plateau provides a complementary validation target from space because it is also homogeneous over large areas, yet it is relatively cold. During summer, cloud-free conditions occur often and the atmospheric humidity is very low with values of total column water vapor around 1 mm. Radiance validation experiments were conducted at |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
title |
Radiometric validation of the Atmospheric Infrared Sounder over the Antarctic Plateau |
spellingShingle |
Radiometric validation of the Atmospheric Infrared Sounder over the Antarctic Plateau |
title_short |
Radiometric validation of the Atmospheric Infrared Sounder over the Antarctic Plateau |
title_full |
Radiometric validation of the Atmospheric Infrared Sounder over the Antarctic Plateau |
title_fullStr |
Radiometric validation of the Atmospheric Infrared Sounder over the Antarctic Plateau |
title_full_unstemmed |
Radiometric validation of the Atmospheric Infrared Sounder over the Antarctic Plateau |
title_sort |
radiometric validation of the atmospheric infrared sounder over the antarctic plateau |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.6761 http://www.webpages.uidaho.edu/~vonw/pubs/waldenetal_2006.pdf |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
http://www.webpages.uidaho.edu/~vonw/pubs/waldenetal_2006.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.6761 http://www.webpages.uidaho.edu/~vonw/pubs/waldenetal_2006.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766268183717609472 |